The majority of research on food webs has focused on temperate lakes, and little is known about the food web of lakes in polar regions. Subarctic lakes are particularly sensitive to climate change, which affects their stability. Therefore, the trophic structure of the
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The majority of research on food webs has focused on temperate lakes, and little is known about the food web of lakes in polar regions. Subarctic lakes are particularly sensitive to climate change, which affects their stability. Therefore, the trophic structure of the food web in such lakes was considered as the object of this study. We studied a clear-water oligotrophic lake located in the subarctic region of Eurasia, specifically in northern Karelia and the White Sea coast of Russia. The study examined both open water periods (summer–autumn) and ice-covered periods (winter–spring) in this lake. Stable isotope analysis of carbon (
13C/
12C ratio or δ
13C value) and nitrogen (
15N/
14N, δ
15N) in producers and consumers was applied and revealed significant seasonal variations in the structure of the food web. The results indicate the presence of both pelagic and littoral/benthic food web compartments, with a notable contribution of autochthonous carbon derived from benthic sources. Omnivorous fish (perch,
Perca fluviatilis; vendace,
Coregonus albula; nine-spined sticklebacks,
Pungitius pungitius) and some benthic invertebrates (mayfly,
Ephemera vulgata; bivalves,
Sphaerium corneum) had intermediate δ
13C values, integrating these compartments by obtaining resources from both. Planktonic invertebrates had significantly depleted
13C, with the lowest δ
13C value reaching −41.7‰, indicating an important contribution of methane-derived carbon. The study also revealed close trophic relationships between lake invertebrates and cyanobacteria, namely with planktonic
Dolichospermum lemmermannii and benthic
Phormidium sp. Seasonal changes in δ
15N values and in trophic position have been observed among predacious omnivorous fish and crustaceans (amphipods,
Gammaracanthus loricatus, and copepods,
Cyclops scutifer), which are capable of a generalist feeding strategy depending on food availability. Using the example of this lake, it can be concluded that polar lake ecosystems are characterized by different seasonal intakes of allochthonous organic carbon from wetland catchment (humic compounds) and nitrogen because of nitrogen fixation in the air by cyanoprocaryotes. Alternative energy sources, such as carbon derived from methane, can also contribute to the energy balance of lake ecosystems. This study contributes to our understanding of energy flow and connectivity between producers and consumers in high-latitude lakes.
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